Dolomitization of the Silurian Niur Formation, Tabas block, east central Iran: Fluid flow and dolomite evolution
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- 作者：A. Mahboubia ; mahboubi@um.ac.ir" class="auth_mail" title="E-mail the corresponding author ; Z. Nowrouzib ; I.S. Al-Aasmc ; R. Moussavi-Haramia ; M.H. Mahmudy-Gharaeia
- 关键词：Hydrothermal dolomitization ; Fluid evolution ; Silurian ; Iran
- 刊名：Marine and Petroleum Geology
- 出版年：2016
- 出版时间：November 2016
- 年：2016
- 卷：77
- 期：Complete
- 页码：791-805
- 全文大小：5998 K
文摘
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Carbonate rocks of the Silurian Niur Formation of east Central Iran were pervasively dolomitized.
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The roles of tectonic setting and thermal conditions for the generation and circulation of dolomitizing fluids as well as formation of dolomite.
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Suggestion a model that shows magmatic activities are related to a late Ordovician to early Silurian rifting phase.